Science · 2005 · 176 citations · 25 references
Natural SciencesEarth SciencesPhysical GeographyClimatologyCryosphere StudiesGlaciologyIce Sheet DynamicsRemote Sensing Of IceGlacier Surface Elevation ChangeIce Sheet Elevation ChangeIce Sheet MonitoringIce Sheet ObservationIce Sheet Thickness ChangeIsostatic UpliftNorth Atlantic Oscillation
A continuous data set of Greenland Ice Sheet altimeter height from European Remote Sensing satellites (ERS-1 and ERS-2), 1992 to 2003, has been analyzed. An increase of 6.4 +/- 0.2 centimeters per year (cm/year) is found in the vast interior areas above 1500 meters, in contrast to previous reports of high-elevation balance. Below 1500 meters, the elevation-change rate is -2.0 +/- 0.9 cm/year, in qualitative agreement with reported thinning in the ice-sheet margins. Averaged over the study area, the increase is 5.4 +/- 0.2 cm/year, or approximately 60 cm over 11 years, or approximately 54 cm when corrected for isostatic uplift. Winter elevation changes are shown to be linked to the North Atlantic Oscillation.
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The NCEP/NCAR 40-Year Reanalysis Project
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